Latest from Svensmark; Forbush events dry out low clouds

Now here is a big deal; episodic CMEs decrease cosmic ray counts at Earth’s surface – AND:

Decreases in Cosmic Rays Affect Atmospheric Aerosols and Clouds

Close passages of coronal mass ejections from the sun are signaled at the Earth’s surface by Forbush decreases in cosmic ray counts. We find that low clouds contain less liquid water following Forbush decreases, and for the most influential events the liquid water in the oceanic atmosphere can diminish by as much as 7%. Cloud water content as gauged by the Special Sensor Microwave/Imager (SSM/I) reaches a minimum ≈7 days after the Forbush minimum in cosmic rays, and so does the fraction of low clouds seen by the Moderate Resolution Imaging Spectroradiometer (MODIS) and in the International Satellite Cloud Climate Project (ISCCP). Parallel observations by the aerosol robotic network AERONET reveal falls in the relative abundance offine aerosol particles which, in normal circumstances, could have evolved into cloud condensation nuclei. Thus a link between the sun, cosmic rays, aerosols and liquid-water clouds appears to exist on a global scale.

Much more can be found here: Forbush decreases confirm cosmoclimatology, and here A link between the Sun, cosmic rays, aerosols, and liquid-water clouds appears to exist on a global scale…,.

A significant conclusion:

Our results show global scale evidence of conspicuous influences of solar variability on cloudiness and aerosols. Irrespective of the detailed mechanism, the loss of ions from the air during FDs reduces the cloud liquid water content over the oceans. So marked is the response to relatively small variations in the total ionization, [that] we suspect that a large fraction of Earth’s clouds could be controlled by ionization. Future work should estimate how large a volume of the Earth’s atmosphere is involved in the ion process that leads to the changes seen in CCN and its importance for the Earth’s radiation budget. From solar activity to cosmic ray ionization to aerosols and liquid-water clouds, a causal chain appears to operate on a global scale.

Why is Pacific cold; and Baja hot?  The role of low clouds in albedo

Why is Pacific cold; and Baja hot? The role of low clouds in albedo

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